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首页> 外文期刊>Canadian Journal of Soil Science >Simulation of soil water dynamics for uncropped ridges and furrows under irrigation conditions.
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Simulation of soil water dynamics for uncropped ridges and furrows under irrigation conditions.

机译:灌溉条件下未耕作的垄沟的土壤水分动力学模拟。

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The ridge-furrow planting system combined with furrow irrigation can effectively increase soil moisture storage and improve water use efficiency in the semi-arid region of China. The precise soil water dynamics in ridge-furrow systems must be known in order to properly design ridge-furrow geometry and improve irrigation uniformity while reducing deep water percolation. The objective of this study was to investigate soil water distribution in the cross-sectional ridge-furrow infiltration, through laboratory experiments and numerical simulations. Six experimental treatments with three soil types (silty clay loam, silt loam, and sandy loam) were tested to monitor both soil water movement and cumulative infiltration in rectangular soil chambers. The HYDRUS-2D model was calibrated and experimentally validated to simulate soil water dynamics. The root mean square error (RMSE) and coefficient of determination (R2) provide a satisfactory quantitative comparison of the goodness-of-fit between observed and simulated cumulative infiltration. The optimized parameters were accurate and the observed and simulated values were very close, which demonstrated HYDRUS-2D as a reliable tool for accurately simulating soil water movement and applied water volume in ridge-furrow irrigation system. In finer soil, the wetted vertical and horizontal distances were equal and soil water distribution was more uniform than that in coarser soil. A high potential of deep water percolation was produced in sandy loam soil. Cumulative infiltration decreased with the increase of initial soil water content, whereas the volume of wetted soil increased with the increase of initial soil water content. Narrow furrows for crops with deep rooting depth and wide furrows for crops with shallow rooting depth were selected in irrigation design. The 40 cm furrow size and higher furrow water depth (water level) were recommended in a ridge-furrow irrigation system.
机译:在半干旱地区,垄沟种植系统与垄沟灌溉相结合可以有效地增加土壤水分存储并提高水分利用效率。为了正确设计垄沟几何形状并提高灌溉均匀性,同时减少深水渗透,必须知道垄沟系统中的精确土壤水分动力学。这项研究的目的是通过实验室实验和数值模拟研究横剖面垄沟入渗中的土壤水分分布。测试了三种土壤类型(粉质黏土壤土,粉质壤土和沙质壤土)的六种实验处理方法,以监测矩形土壤室内的土壤水分运动和累积入渗。对HYDRUS-2D模型进行了校准和实验验证,以模拟土壤水分动力学。均方根误差(RMSE)和测定系数(R 2 )提供了令人满意的定量比较,该观测值与模拟累积渗透之间的拟合优度有关。优化的参数准确,观测值和模拟值非常接近,这表明HYDRUS-2D是准确模拟垄沟灌溉系统中土壤水分运动和施水量的可靠工具。在较细的土壤中,湿润的垂直和水平距离相等,并且土壤水的分布比在较粗的土壤中更均匀。沙质壤土产生了很高的深层水渗透潜力。累积入渗量随初始土壤含水量的增加而减小,而湿润土壤的体积随初始土壤含水量的增加而增加。在灌溉设计中,选择了生根较深的作物的窄沟和生根较浅的作物的宽沟。在垄沟灌溉系统中,建议沟长为40厘米,沟水深度较高(水位)。

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